Premier Tours : Seward to Anchorage Alaska

Seward Population: 2,693 Located on , approximately 127 miles south of Anchorage, Seward is known as the “Gateway to Kenai Fjords National Park”. It was founded in 1903 as the southern terminus of the .

One of only two deep-water ports south of Anchorage, Seward is the port for the two Royal Caribbean and Celebrity cruise ships. The bustling harbor and historic downtown district is filled with quaint shops and art galleries. The Port of Seward is also an important seafood shipment center, handling halibut, salmon, and crabs. According to a 2011 National Marine Fisheries Service report, Seward is the ninth most lucrative fisheries port in the United States based on the monetary value of fish taken from the port.

In the summer months, visitors come to experience trophy sport fishing, glacier and wildlife cruises, sailing, hiking, kayaking, flightseeing, summer dog sled rides, and more. In winter, Seward transforms itself into a winter wonderland offering cross-country skiing and snowmachining adventures.

The City of Seward is named in honor of William Henry Seward. He served as the United States Secretary of State during the administrations of Presidents Abraham Lincoln and Andrew Johnson. As secretary of state, Seward negotiated the United States purchase of Alaska from Russia in 1867. The treaty was signed March 30, 1867, and is celebrated annually as Seward’s Day.

Resurrection Bay was named by Russian fur trader and explorer Alexander Baranof, in 1791. While sailing from Kodiak to Yakutat, Baranof encountered a storm and found shelter in this bay on Russian holiday of the Resurrection, Baranof named it accordingly. Resurrection Bay remains ice free all winter.

Summer average temperature is 62 degrees. Winter average temperature is 18 degrees. Average rainfall is 60 inches. Average snowfall is 80 inches.

Today in Seward The seasonal economy during the summer is based around fishing and tourism. Seward’s year round economy is based on the port (shipment of coal and freight), the prison and the research of the marine life. The unemployment varies from 18% in the winter to 5% during the summer.

Seward has a city sales tax of 5%. The fire department has 2 full time workers and 32 volunteers. Police Department has a chief with 7 officers. About 600 kids go to school from grades K-12. Hospital has 33 beds.

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Polar Bear Jump The Polar Bear Jump is a weekend event held in January, when several costumed characters plunge into Resurrection Bay to raise money for the American Cancer Society and the Children with Cancer. Weekend events include a bone-chilling parade, bachelor/bachelorette auction, waiter/waitress contest, and oyster slurping. This year, over 150 jumpers, along with related activities raised over $170,000 to battle cancer. The first Polar Bear Jump was held in 1986. Jackpot Halibut Tournament The Jackpot Halibut Tournament is held every year from mid-May through mid- September. Prizes are awarded each week of the tournament for various categories, largest fish, tagged fish, and even a left-handed caught fish award. Prizes are also awarded based on random target weights ranging from 60 to 120 pounds. A grand prize jackpot winner is determined at the end of the tournament. In 2011, Chad Aldridge won the Jackpot prize of $28,260.00 for the largest catch during the season that weighed in at 350.8 lbs.

Mt. Marathon Race The Mt. Marathon race is held every year on the fourth of July. The Race, according to folklore, began when two sourdoughs had an argument about whether it was possible to climb and descend the mountain in less than one hour. “Impossible”, one said. To settle the argument and the resulting wager, it was decided to hold a race with the loser to furnish drinks for the crowd.

The race is just 265 feet short of three miles, but is 3,022 feet straight up and the medics are ready and waiting as the runners come across the finish line. While short, it is grueling with an often muddy and treacherous trail.

The current record for men is 43 minutes, 23 seconds, set in 1981 by Bill Spencer, a member of the 1988 Winter Olympic Ski Team. The fastest woman is Nancy Pease, who ran it in 50 minutes, 30 seconds in 1990. Olympic cross-country skier Nina Kemppel is the record-holder for the most wins – eight.

For safety reasons only 200 entrants are allowed for each race and registration begins in January. There is a race for men, women, and children. In 2011, Eric Strabel of Palmer, Alaska won the race in 44 minutes, 40 seconds for the men division. Kikkan Randall of Anchorage took the women’s division with a time of 52 minutes and 3 seconds.

Silver Salmon Derby This event is held in August. Every year the derby offers a $10,000 prize for the biggest fish, but there is ample cash and other prizes for all of the top 50 salmon. Last year’s winner was Phillip Lazenby of Kenai, Alaska. His 19.15 pound coho (silver salmon) won him $10,000 for first place.

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The Effects of the Good Friday 1964 Earthquake on Seward The earthquake was a defining moment in Seward’s history. Thirteen people died – mostly due to the tsunamis that followed the 9.2 quake. Eighty-six homes were demolished and hundreds of others damaged. Seward’s waterfront industry was destroyed: docks, railroad, fish processors, oil companies, and most of the fishing fleet. From its founding in 1903, the town had served as a transportation hub with its marine, rail, and, later, highway links to other points in Alaska. The earthquake severed all these connections, and it took years for the community to rebuild its economic base.

Oil storage tanks along Resurrection Bay exploded and caught fire. Afraid Seward would be consumed in flames, people headed out of town, but the first bridge over Resurrection River had sunk five feet and was impassable. There was no way out. The quake also loosened huge amounts of silt that flowed into the bay. As the sea bottom heaved and dropped, a huge whirlpool developed and water drained into the void. The Alaska Standard, a docked oil tanker, hit bottom. Vast portions of the waterfront, 50 to 400 feet wide, simply fell into the water.

The first tsunami, as wide as the bay, and perhaps 30 feet high, rolled in about 30 minutes after the quake began. Wave after wave continued, and did not stop until the following morning. As testimony to its strong spirit and for the way its residents pulled together after the quake, Seward was recognized as an All-American City in 1965.

Seward Coal Terminal In late 1984, a new $22 million coal-loading facility was opened in Seward for the purpose of moving coal brought by train from interior Alaska to ships bound for South Korea. The Koreans used the Alaska coal to produce electricity for the Korean Electric Power Corporation. Until 2002, the Usibelli Coal Mine, located about 90 miles south of Fairbanks, provided approximately 800,000 tons of coal each year to Korea. (See Usibelli Coal Mine commentary)

Shoreline Information and Marine History Alaska has about 34,000 miles of total shoreline. That is more shoreline than the combined shoreline of the “Lower 48”. Though highways cover only about one-third of Alaska, state officials estimate that 95% of Alaska’s residents are accessible by commercial marine carriers. Alaska waterways have been a major part of its history since the beginning. A brief Marine History:

• 1775 – 1825 Russian hunters and traders took over 200,000 sea otter pelts from Alaska • 1778 – 1790s Explorers James Cook and George Vancouver charted the

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Pacific coast and worked their way into looking for the Northwest Passage to the Atlantic Ocean • 1870s Boasts used to transport ore from the Copper River Delta moved furs from and shuttled goods and people during the Gold rush of late 1800s. • 1963 Regular state ferry service to started

Located near the major Great Circle shipping routes, Seward has the ideal location for Alaskan shipping. Until recent years, vessels in need of repair had to make the long and expensive journey to Vancouver or Seattle, but now most repairs and scheduled maintenance can be performed in Seward. Seward’s Maine Industrial Center has nearly 1,000 feet of dock space, including a 350-foot synchrolift dry dock capable of handling vessels up to 3,600 tons.

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Mile 0 of the Seward Highway Alaska SeaLife Center The Sea Life Center is a cold water marine science facility and it’s mission is to combine research with wildlife rehabilitation and public education. It opened in 1998 with money from grants, bonds, donations, and fines from the Exxon Valdez oil spill.

They take in orphan animals and stabilize them to be released back into the wild or transferred to a new home. Over the past year their “patients” have included: Sea Otters, Harbor Seals, Stellar Sea Lions and over a dozen birds.

Research is currently being done to learn more about the local marine birds and wildlife. The main research going on right now is to find out why the Stellar Sea Lions and the Sea Otters population in the Gulf of Alaska region are declining so quickly.

Heading out of Seward toward Anchorage

Mile 2 Seward Chamber of Commerce Visitor Center

Spring Creek Correctional Facility The Spring Creek Correctional Facility is the only maximum-security facility in Alaska. The institution has a capacity of over 500 male inmates and employs more than 200 staff. Its mission is to operate a maximum-security facility, placing the highest priority on public safety while providing a secure and humane environment for offenders, staff, and visitors.

Mile 3 Resurrection River The bridge over Resurrection River is the geographic city limits for the city of Seward. The river’s water source is the Harding Ice Field and explains why the river is “dirty” with glacier silt.

The Seward Highway The Seward Highway follows the route of an old mail trail, the Johnson Trail, which was built paralleling the north shore of the . In 1915, the Crow and India n Pass trails were in heavy use as supply routes to the Iditarod gold fields in interi or Ala ska .

Construction began on the highway after WWII in 1948 and was completed in 1950. The highway was not paved until 1954. Improvements are continuously being made on the road as travel increases between Anchorage and the Kenai Peninsula.

The Seward Highway runs 127 miles from Seward to Anchorage and has been designated an All-American Road and National Forest Scenic Byway.

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Mile 3.7 Exit Glacier Road Exit Glacier Exit Glacier in the Kenai Fjords National Park is just 10 miles north of Seward, and is the easiest to reach of the many glaciers that flow from the Harding Ice Field. Exit Glacier Road takes you to the Ranger Station and picnic site, only a half of a mile from the glacie r. Trails lead you to the glacier and your choice of either a ¾ or 3.5 mile hike a round the area. Exit Glacier is a remnant of a larger glacier once extending to Resurrection Bay.

Mile 17.7 Once know as Long Lake, is approximately 24 miles long, less than 2 miles wide and is almost 800 feet at its deepest point. It is one of the largest lakes in Alaska. The lake is glacially carved and is fed by the Harding Ice Field and mountain runoff. The turquoise color of the water is a result of the sun light reflecting off of the suspended glacier silt particles in the water. Kenai Lake serves as the headwater for the Kenai River, which provides south central Alaska with some of the best fishing in the state. Famous for its King Salmon, the largest King Salmon caught here was in 1985, weighing 97.4 pounds. The Kenai River flows 75 miles before entering Cook Inlet.

Mile 20 I.R.B.I. Knives You’ll notice the big knife outside. “I’d rather be independent” knife shop houses an impressive collection of hand crafted knives.

Mile 23.1 Ptarmigan Creek

Mile 24.2 Lower Trail River

Mile 26 Lower Trail Lake At one time there was a gold and quartz mine to the east. This area is great for camping and hiking and there are several state operated camp sites nearby. The lakes here are popular with the float plane pilots and fly out fishermen. The have a nice population of trout and salmon. In the late summer, this is a good spot to look for wildlife that feed on the spawned salmon.

Mile 29.4 Moose Pass Moose Pass is a small, isolated community home to about 219 full time residents. It currently serves as a highway maintenance station for this section of the road.

In its former days, this mountain village on Upper Trail Lake was a construction camp on the Alaska Railroad. By 1908 the construction of the railroad had made its way to Moose Pass. Though no rail cars were traveling the lines, it provided a way for pack animals and dog teams to make their way to the gold fields.

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The naming of Moose Pass has a couple different origins. One story says in 1903, a mail carrier driving a team of dogs had considerable trouble gaining the right-of-way from a giant moose. Local resident Ed Estes attributes the name Moose Pass to a 1904 observation by Nate White of the first moose recorded in this area.

Both stories give some character to the town famous for its waterwheel that turns a grindstone, built by Estes, that claims “Moose Pass is a peaceful little town. If you have an ax to grind, do it here.”

Mile 32.4 Trail Lakes Fish Hatchery The Trail Lakes Fish Hatchery is open to visitors year round and is run by the Cook Inlet Aquaculture Association. They raise sockeye (red) and coho (silver) salmon here as a way to enhance the salmon run that takes place each season in the nearby streams and lakes.

Spruce Bark Beetles The forest in the Moose Pass/Trail Lake area consists primarily of mature spruce and hemlock with pockets of birch.

The spruce trees in this region are being attacked by a tiny beetle known as the spruce bark beetle. Infested trees take on an orange to reddish hue about one year after beetles enter the soft inner bark layer to lay their eggs. In turn, the damage to the trees is not caused by the adult beetle but rather the larvae. Larval feeding eventually destroys this layer of bark that transports tree nutrients from the roots to the outer part of the tree. Spruce beetle outbreaks stunts the growth of trees and can cause tree mortality.

While the spruce beetle is a natural part of the forest ecosystem, a massive spruce beetle outbreak has killed mature spruce trees on one million acres of the Kenai Peninsula since the mid-70’s. That equals about 50% of the peninsula’s forested land. Climate change in the region (hotter/drier conditions) is cited as the reason for the beetle outbreak.

Mile 36.4 Avalanche gates The beautiful mountains in this area 3,000 – 5,000 feet above sea level and provide excellent opportunities for outdoor activities. While these mountains provide pleasure, their steepness also adds an element of danger during the winter season.

Avalanches have taken numerous human lives in the past and have destroyed property along the Seward Highway. To prevent these avalanches from occurring at unpredictable times, the Forest Service has a system in which they control the fall of the avalanche snow. Avalanche control is the scientific method of triggering an avalanche before it

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becomes a danger. While avalanches are somewhat predictable due to snow conditions and temperature, the Forest Service prevents them when necessary.

Using the arm crossings to close the road (similar to RR crossing arms) the Forest Service mounts a 105-mm Howitzer (a rifle), borrowed from the military, on the platforms located at various points along the highway. The platforms are the rust colored culverts with the platform across the top of the culvert. The recoilless rifle fires a shell int o the side of a dangerous slope and releases the snow and lets the avalanche run its course without the potential of injuring people or destroying property. The road is then cleared and reopened to the public. Because this is the only road between Anchorage and the Kenai Peninsula, the road is maintained all winter long.

Mile 37 Tern Lake Junction – End of Alaska Route 9 Just north of Tern Lake is the junction for Cooper Landing and . Good place for bird watching, especially for the Arctic Tern. They are easy to spot with their forked tails, black heads and aerial acrobats. They search for small fish from the air and then dive into the lakes or ponds. They migrate thousands of miles each summer from Argentina and Antarctica, making them the longest migratory birds in the world.

Mile 39.4 Devil’s Pass Trailhead Part of the Resurrection Pass Trail system. A 10 mile hike to the main trail between Hope and Cooper Landing.

Miles 39.6 & 43.8 Avalanche Gates

Mile 45.5 Summit Lake

Mile 47.2 Lower Summit Lake

Mile 48 Approved Stop No bathrooms. No snacks or drinks.

Mile 56.6 Junction Hope and Sunrise This is the turnoff for the town of Hope. Hope is a historic mining community. On the road to Hope, the old gold mining town of Sunrise City was located at Six Mile Creek. During the gold rush era of 1896, an estimated one million dollars of gold was mined at Sunrise and Six Mile Creek. At that time, the area had a population of 3,000 people. Today the town of Sunrise is a ghost town where not a single building remains.

Hope is located at the end of the road about 17 miles off of the main highway. Unlike Sunrise, many of the original buildings remain in use in Hope. It is the site of the oldest

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school house in Alaska. With a population of approximately 192 people, Hope is a favorite summer fishing spot. Hope also serves as the head of the 78 mile Resurrection Pass Trail, which crosses the Kenai Mountains and ends in Sterling.

Mile 57 Canyon Creek Bridge (over Six Mile Creek) Approved stop. Bathrooms available, no snacks or drinks. Six Mile Creek is a popular rafting and kayaking spot for visitors and locals. The rapids are rated at Class IV and V due to the narrow, steep-walled canyons that can make passage difficult.

Mile 63.3 Granite Creek Bridge – Halfway Point between Seward & Anchorage

Mile 68.5 Turnagain Pass Recreation Area Elevation: 988 feet Approved stop. Bathrooms available. No snacks or drinks. Driving through the Turnagain Pass, the highway is lined with western hemlocks. These trees grow in conjunction with the Sitka Spruce. The absence of the lower branches is due to the snow blowers that keep this road clear during the wintertime.

On top of the pass, tree line reaches its highest point at about 1500 feet above sea level . Beyond that point, the mountains are covered with a mixture of low-lying plants, shrubs, grasses and tundra carpet.

Snow accumulation in the Turnagain Pass region falls in excess of twenty feet during a good winter. You can notice a large pole to measure the depth of the snow at the top of the pass. The deep snow provides locals with the huge winter playground from November until early April. To accommodate all the different types of winter recreational users, the highway has been divided with the west side of the highway devoted strictly to snow-machining and the east side is designated as the cross-country ski side. By separating these two recreations, each group can enjoy their sport at their leisure.

Mile 75 Pullout at the bottom of Turnagain Pass, watch for blueberries Approved stop. Bathrooms available, no snacks or drinks

Mile 75.2 Ingram Creek Originally named Quartz Creek, the creek was renamed after R.C. Ingram, an engineer with the Bureau of Public Roads. Ingram Creek drains into the Turnagain Arm and was famous in the time of the gold rush. In 1898, when gold prospectors and US Army exploration teams came through Portage Pass, Quartz Camp developed into a gathering site among people. Boat service from Sunrise City to the camp and back was offered during the Gold Rush. About 400 miners located themselves at Quartz Camp in May of 1898 waiting to take advantage of the gold that had been discovered in Hope and Sunrise.

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Kenai Peninsula The Kenai Peninsula is 150 miles long and 70 miles wide. Many people consider the Kenai “Anchorage’s Playground”.

1957 oil and gas reserves were discovered by Atlantic Richfield. The oil lies about three miles below the surface near the headwaters on the Swanson River 20 miles northeast of Kenai (city). About 70,000 barrels per day of crude and 630,000 cubic feet of gas per day are within the Kenai and Cook Inlet region.

Mile 77 Boundary to Turnagain Arm Reaching the beginning of the Turnagain Arm, which is referred to as an isthmus, looking to the east one can see the tops of the mountains that form the divide between Prince William Sound, the Portage Valley and Turnagain Arm. At this point only 12 miles separates the Portage area from Prince William Sound. Had glaciers carved those 12 mile s further inland connecting Prince William Sound with the Turnagain Arm, the Kenai Peninsula would actually be an island with over ten thousand square miles in land.

Millions of years ago, glaciers and ice fields covered the south central valley, carving valleys and different formations. As the 3,000 feet of ice and glaciers receded, Turnagain Arm, a shallow arm of the ocean that is fed by glacial meltwater, was created. While this body of water is referred to as an arm, the proper term is fjord, which is a glacial valley that has been submerged with seawater.

Turnagain Arm, approximately 48 miles long, is a shallow fjord of the upper Cook Inlet. This salt-water arm separates the Kenai Mountains to the south from the to the north along the highway. In reality, the Chugach and Kenai Mountains are the same geological structure, but glaciers carved a deep trough that today separates the two mountain ranges.

A few years ago, a road development crew drilled deep into the Turnagain Arm to estimate how far down they would have to develop the area in order to build a bridge across the arm. The crew drilled down 3000 feet and never hit solid ground. Thus, the idea of a road connecting each side of the arm was dismissed and continued construction of the current road (the Seward Highway) replaced the idea.

Turnagain Arm Discovery Although the Turnagain arm developed into a popular route for early Russian fur traders and Alaska Natives, Western Europeans only discovered the Turnagain Arm after Captain James Cook sailed into this area of Alaska in 1778.

In search of the Northwest Passage, a passageway connecting the Pacific Ocean to the Atlantic Ocean, Captain Cook sailed one of his ships, the Resolution, into this area. As

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he made his way up the arm, Captain Cook soon discovered that the body of water was not the Northwest Passage but rather a river of some sort as he could not see furthe r inla nd. After his revelation, Cook had to “turn again” to safely get his ship out of the arm in his quest for an alternate route to Asia.

After hearing of Captain Cook’s discovery, Captain George Vancouver, an extremely knowledgeable navigator, retraced Captain Cook’s voyage up “Cook’s River” and discovered that the river was indeed an arm of the sea. From that point on, British maps showed the body of water as Turnagain Arm. Turnagain Arm drains into the Gulf of Alaska and then finally into the Pacific Ocean.

Mile 78.9 Road Turn off for Portage Glacier and the town of Whittier.

Whittier Whittier has about 220 people living in this quirky little community. It started as a construction camp for the Army during the construction of the tunnels for the Alaska Railroad. They were stationed there until 1960. The 1964 earthquake damaged most of the buildings.

Now almost the entire town lives under one roof – earning the nickname “The city under one roof”. They all live in one large building made up of condos. Most everything the people of Whittier will need (groceries, etc.) is found in that one building. Because of the high winds Whittier experiences, there is an underground tunnel that connects the building to the school, so children can get back and forth safely each day. The economy is based around tourism and fishing. It is also the gateway to the western part of Prince William Sound.

Portage Train Station The tunnel system was constructed from 1941-1943 by the Army Corp of Engineers, headed by a man named Anton Anderson. On April 23, 1943 workers completed the spur, which consisted of a 1-mile tunnel through Begich Peak and a 2.5-mile tunnel through Maynard Mountain. It was important to have access to Whittier, another deep water port, during WWII in case the Japanese bombed the port of Seward.

They chose Whittier because of the weather and landscape. Most days Whittier has low clouds and rain and sits on the west side of Prince William Sound against the Chugach Mountains. This location made it hard for Japanese aircraft to spot the tracks most days.

Until 2000 the train was the only way to get to the community of Whittier. The 2.5 mile railroad tunnel was converted to make vehicle traffic possible beginning in June, 2000. Named for the head engineer during its construction phase, the Anton Anderson Memorial Tunnel is only wide enough to allow one-way traffic. Because of this, all

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traffic to and from Whittier is regulated by the tunnel schedule. During the summer, the tunnel is opened 5:30am to 11:15pm, with tunnel openings on both ends occurring each hour.

Facts about the Anton Anderson Memorial Tunnel

• Longest highway tunnel in North America (13,300' or 2.5 miles).

• Longest combined rail and highway use tunnel in North America.

• First U.S. tunnel with jet turbine and portal fan ventilation.

• First computerized regulation of both rail and highway traffic.

• First tunnel designed for -40° F and 150 mph winds.

• Portal buildings designed to withstand avalanches.

Mile 79 Alaska Wildlife Conservation Center (Big Game Alaska) Located on 140 acres, AWCC opened to the public in 1993. They provide care for injured and orphaned wildlife and provide continued wildlife awareness and education to the public. Visitors have close encounters with moose, bison, elk, muskox, caribou, Sitka black- tailed deer, and birds of prey. All proceeds from sales at the gift shop and snack bar go back into the program for continued wildlife care and protection.

Mile 80 Portage Portage is named because it was a short portage of 10 miles across the mountains to Prince William Sound. The proximity of Turnagain Arm and Prince William Sound has created a meteorological dynamo. The weather here is harsh with violent winds, heavy rain and snow. The small community of Portage once had 75 residents, but is now a ghost town. The culprit was the 1964 earthquake when it dropped this land over 5ft, flooding homes during extreme high tides. You can see what is left on the side of the road across from the train depot. Most people accepted land from the government to move to higher ground.

Mile 81 Twenty-Mile River Observation Platform, Hooligan Fishing Smelt are a common sight during May in the creeks along the highway. When crossing Twenty-Mile Creek, look for people throwing nets into the water. Hooligan, also known as candlefish, is one of five species of the smelt family found in Alaska. Candlefish are caught, dried and because they are so oily they can be fitted with a wick and burned exactly like a candle.

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Mile 89.1 Virgin Creek - View of three glaciers to the east

Evidence of Earthquake next 15 Miles Prior to the spring of 1964, the upper end of Turnagain Arm supported a lush community of succulent willow thickets and freshwater marshes with stands of tall cottonwoods. Moose and waterfowl were frequently seen in high numbers in the area. On March 27, 1964 this area was drastically altered in a matter of moments. The most powerful earthquake ever recorded in North America rumbled through the region registering 9.2 on the Richter Scale. In south central Alaska, the quake killed an estimated 115 people and extensively damaged communities throughout the region. The epicenter of the earthquake was located near Miner’s Lake, which is west of Columbia Glacier in Prince William Sound.

Remnants of houses from the old town of Portage are still visible on the west side of the highway across from the train station. Railroad tracks were twisted and bent while buildings and bridges collapsed and roads became a ruin of cracked slabs. Land to the west of the glacier sank up to 8 feet drowning shoreline forests, and land to the east and south of the epicenter rose to an extreme of 35 feet. The east end of Turnagain Arm sunk and the tidal waters and silt killed the cottonwoods and willows and transformed the marshes into silty, saltwater mud flats. Wildlife abandoned the area for the most part, but has returned.

Mile 90 Alyeska Highway - Girdwood Girdwood, originally named Glacier City, was founded as a gold mining town at the turn of the century with several gold claims being staked on Crow Creek and the Virgin and California Creek drainages. As the number of miners increased, a supply camp arose that also supplied a trail stop on the route between Seward and Ship Creek which is now Anchorage.

James Girdwood was an Irish immigrant and linen merchant with four gold claims on Crow Creek. He later became the namesake for this mountain community. Though founded as a mining town, the development of Girdwood was spurred by railroad construction begun by the Federal Government in 1915. The little town boomed with new businesses. Mining in the upper Crow Creek area continued into the late 1930s when mine closures by a World War II presidential order made Girdwood a near ghost town.

In 1949, Girdwood again flourished as construction began on the Seward Highway connecting the seaport of Seward to Anchorage. In 1954, eleven local men formed the Alyeska Ski Corporation with dreams of establishing a first-class ski resort. In 1960, the first chair lift and a day lodge were built. Francoise de Gunzburg, a Frenchman and a member of the Rothechild Banking family managed to secure a used chair lift from France that was dismantled, shipped to Alaska and rebuilt at Alyeska.

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Then, tragedy struck. On Good Friday in 1964, an earthquake with the magnitude of 9.2 dropped the coastal edges along the Turnagain Arm 8 to 10 feet! Consequently, the townsite of Girdwood moved two and ½ miles up the valley to the present location. Three years later, the resort was sold to Alaska Airlines and the present General Manager, Chris von Imhof, then the Director of Tourism for the State of Alaska, was hired to run the resort.

The Nugget Inn, the original hotel, was built and a second chair lift was constructed on the upper mountain. Finally, in October 1980, Seibu Corporation, a Japanese company, purchased the Alyeska Resort and invested heavily in its development. Seibu built a new high-speed quad chair, a fixed quad and a 60 passenger aerial tramway. In addition to the ski resort, the Alyeska Prince Resort, a luxurious 307-room hotel, was opened in Augus t of 1994. The hotel was sold in 2006 to a private investor and is now called The Hotel Alyeska.

After the 1964 Earthquake the town-site was also moved up the valley 2.5 miles to its present day location at the junction of Alyeska & Hightower Roads. The original town- site was close to the Tesoro Gas Station along the highway.

The Hotel Alyeska The Hotel Alyeska, the largest ski resort in Alaska, is located approximately 40 mile s sout h of Anchorage. Home to Olympic Gold Medalist Tommy Moe, Alyeska has some of the most challenging terrain for a Western United States resort. Although Alyeska doe s not have a large amount of lifts or runs, the vertical feet is what makes the skiing challenging.

The hotel hosted the 2007 US Alpine Championships. They also hosted the event in 1981 and in 2004.

Alyeska, which is an Aleut word for “great land of white to the east”, typically, receives over 20 feet of snow annually. The elevation at the base of the mountain is 280 feet and at the top the elevation is 3,939 feet above sea level. Alyeska is the only resort in the US that climbs directly from sea level.

Facilities on the mountain include 4 double chairs, 1 quad chair, and a 60 passenger aerial tram that is located at the base of The Hotel Alyeska. Along with the beautiful hotel, the mountain also has two base lodges and a lodge at the top of the tram. Operations of the tram are year round and Alyeska boasts one of the best views from the top of any ski re sort in the United States.

Some people from Anchorage have condos in Girdwood and can access the mountain in about an hour from Anchorage. Alyeska provides visitors with many different activities

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during both the summer and winter months such as the Spring Carnival and the Fall Festival. Alyeska is also a great day trip from Anchorage.

Sitka Spruce Around Girdwood, surrounding the highway are Sitka Spruce trees. Sitka Spruce, the state tree of Alaska, is a dark, heavy-limbed conifer with branches lifting upward towards the sky rather than hanging down like the white spruce tree. Sitka Spruce was an important wood during the early part of WWII when light planes were constructed from the trees straight-grained wood. Sitka Spruce also played a vital role in the building of the Alaska Railroad as the coastal forest provided fuel, cabin logs, and construction materials.

Mile 90.4 Chugach National Forest (Forest goes south to Seward) (Park goes north to Anchorage) Chugach National Forest Chugach National Forest is the second largest national forest in the US. (The first largest national forest is also located in Alaska, Tongass National Forest in southeast Alaska.) The Chugach National Forest is nearly five million acres in size and occupies nearly all of the forest scenery across the arm. The Tongass is over 3 times its size 17+milli on acre s. The National Park was established 16 years after the National Forest System Act was signed into law in 1891. The name, Chugach, comes from an Eskimo tribal name that means ‘rainmakers’. The mountain range is still known by the same name.

Chugach State Park At 495,000 acres, it is America’s third largest State Park. It was established in 1970 and provides easy access to both visitors and residents who want to hike, ski, camp, view wildlife and take part in many different outdoor activities. Chugach State Park blends into the boundaries of Chugach National Forest.

Alaska’s State Park system was started in 1959 and encompasses more than 3 million acres around the state. The largest state park in the U.S. is Wood Tikchik State Park located about 500 miles west of Anchorage and directly north of Dillingham.

Mile 90.8 Railroad crossing, the Alaska Railroad The Alaska Railroad, the northernmost railroad in the United Sates, begins in Seward, follows the Turnagain Arm, and ends within 120 miles of the Arctic Circle in Fairbanks. While the railroad covers quite a few miles, the only route is in the corridor between Seward and Fairbanks.

With construction of the railroad beginning in 1915, the job took approximately 5,000 people and about eight years to complete, it was done in 1923. Financed and constructed by the federal government, the railroad tab totaled $56,000,000 or $78,000 per mile.

15 Premier Alaska Tours Seward Highway: Seward to Anchorage Alaska

Although the Seward Highway serves as the main thoroughfare from Anchorage to Seward, prior to the construction of the highway, the train was the only way to reach Seward and other areas of the Kenai Peninsula.

Mile 101.3 Bird Creek Many of the rivers and creeks along the road are home to Alaska’s various species of salmon. The glacial silt does not affect the salmon as they migrate from the salt water to the fresh water streams. The most common salmon in these waters are the Coho or Silver Salmon. They are usually in the streams in mid-summer, especially around Bird Creek. The Arm and streams are also home to the Chinook/King and Pink/Humpy salmon.

Mile 103 Indian Creek, Town of Indian On this side of the Turnagain Arm, gold mining in the area of Indian also surfaced. Prospectors moved from Sunrise and Hope as the gold depleted and found fortune in the creeks that drain into the Turnagain Arm. The sites of Indian, Bird Creek, Girdwood, and Crow Pass are remnants of the gold rush. Indian Creek developed into the site of a sawmill and a roadhouse to serve hardy travelers cutting through the Chugach Mountains towards the interior gold fields.

Indian Valley, an original part of the Iditarod Trail, served as the mail route and an alternate route used in later years. Indian also served as an important wood supply center for the construction of the Alaska Railroad. In 1918, the Alaska Engineering Commission built a sawmill at Indian which burned in an arson fire soon after. The Commission turned to the community of Indian for their need of wood immediately and relied on local residents for their supply. While Indian no longer serves as an area to find gold or buy wood, much of Anchorage’s meat is processed in this area at Indian Valley Meats. Indian Valley Meats process reindeer sausage, smoked salmon and custom meat products.

Mile 104 Indian Valley Mine National Historical Site The Indian Valley Mine is locally significant for its association with lode mining and early settlement on the Turnagain Arm during the years of 1920-1939. The Cabin and Assay building are the oldest structures on the Turnagain Arm and are listed as a National Historic Site. People can visit the museum and pan for gold.

Mile 106.6 Watch for Dall Sheep Located on the cliffs of the Chugach State Park are Dall sheep. Dall sheep are usually spotted on the south side of Beluga Point in either the Cliffs or right next to the road. The sheep that are seen just outside of Anchorage are part of a heard of several hundred that live in Chugach State Park.

Named for William H. Dall, one of the first men to survey the lower in 1866, Dall sheep are sometimes referred to as Alaska bighorn sheep because the Rocky Mountain

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bighorn are a closely related species. Rams, noticeable by their bright white color, grow large cured horns formed from a specialized skin structure made up of a compacted mass of hair and oil. The horns are not shed each fall but instead the sheep add another ring to their horns yearly so the longer the horns, the older the ram, and thus the more dominant that ram is within the herd.

The rams can weigh as much as 300 pounds with the female sheep, ewes, weighing around 150 pounds. The Dall sheep make their home in the high alpine tundra and subsist on grasses, mosses, lichens, and flowers. Dall sheep have excellent sight and their climbing ability keeps their enemies at a far distance. Roughly 60,000 to 80,000 Dall sheep reside in the Chugach, Kenai, Alaska and Wrangell mountain ranges in Alaska. During the summer, the rams migrate high into the ranges, leaving the prime lower grazing grounds for the ewes and lambs.

Mile 110.3 Beluga Point, watch for Beluga Whales Due to the density of silt in the Turnagain Arm, no sunlight penetrates through the water. Without sunlight, the process of photosynthesis cannot occur and without photosynthesis, no animal life, not even plankton can exist in the Arm. Thus, the Turnagain Arm is literally lifeless, yet the streams that feed the Arm contain salmon.

To get to their spawning beds, the salmon must swim from the ocean through the Turnagain Arm up to their spawning streams. Following the salmon into the Arm each year are the beluga whales. Beluga whales, which in Russian means “white”, are a small toothed whale that looks much like an oversized dolphin. An adult male can weigh 2,000 pounds and reach 15 feet in length. Their life expectancy reaches about 40 years.

Glacial Silt The sand-like material surrounding the Turnagain Arm is glacial silt or rock flour. Although the silt beaches surrounding the Turnagain Arm look enticing on warm days, the silt is extremely dangerous. When mixed with the right amount of water, the silt acts like quicksand and has the potential to trap whatever happens to walk on it. Advisories are posted along the Arm warning people of the dangers of silt.

Bore Tides Another phenomena of the Turnagain Arm are the bore tides that roll through the arm periodically. While the Turnagain Arm has the second highest tide in North America, the arm also has the opposite extreme lows. These diurnal tides, two high tides and two low tides in a 24-hour period, keep the Turnagain Arm in constant motion.

A tidal bore is a high, abrupt tidal wave that occurs in a narrow, tapering channel where tidal changes are extreme. Because Turnagain Arm is relatively shallow and is a constricted arm of the sea adjacent to a deeper body of water with a large range in tides, these bore tides occur. Bore tides, known to occur in only 67 places around the world,

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reach amazing heights and remarkable velocity. Bore tides towering as high as 26 feet and traveling up to 24 miles per hour have been recorded in different parts of the world.

Turnagain Arm is one of the few locations where a bore tide occurs regularly in the U.S. The statistics for bore tides in the Turnagain Arm are: • Range in size from ½ foot to 6 feet high • Travel up to 15 miles per hour • Occur daily, usually 1 ¾ to 2 ½ hours after the predicted low tide in Anchorage. • Opposing wind can increase visibility of bore tides.

Surrounding Mountains of Turnagain Arm As you travel north from Seward, located to the north are the Chugach Mountains which are part of Chugach State Park. On the cliffs of the park, rock climbers are often spotted in the summer as well as hikers and mountain bikers. Located to the south are the Kenai Mountains which range in height from 2,000 feet to 6,000 feet.

On a clear day, the is visible to the west. The Alaska Range, whic h include s Mt. McKinley, forms an arc that spreads across the middle of the state. Some of the more visible mountains in the Alaska Range are the volcanoes Mt. Redoubt and Mt. Spurr, seen across Cook Inlet. Also, Mt. Foraker and Mt. Hunter which can be seen to the left of Mt. McKinley.

While this chain of mountains is volcanically active, only in recent years has the south central region experienced any eruptions. Some geologists consider Mt. Spurr to be the northern terminus of the Aleutian Range, which is volcanic. That is how geologists differentiate between the Aleutians and the Alaska Range, which is not volcanic.

In December of 1989, Mt. Redoubt erupted and sent an ash plume over 40,000 feet into the air. Again in 1992, Redoubt erupted and laid a blanket of ash over the Anchorage area and caused major delays both on the ground and in the air. (See more information on volcanoes in the Miscellaneous Information section of this commentary.)

Quick Mountain Facts: Average elevation in the Alaska Range: 7,500 feet. 3 highest peaks in the Alaska Range: McKinley (20,320), Foraker (17,400) and Hunter (14,573). Aleutian Range is the SW continuation of the Alaska Range. Average elevation in the Aleutian Range: 5,000 feet. 4 higheast peaks in the Aleutian Range: Spurr - closest to Anchorage (11,066), Redoubt – across from Kenai (10,197), Iliamna – NW of Homer (10,016) and Augustine – SW of Homer (4,206), all of which are volcanic and have erupted since the 1950s.

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Mile 115.3 Potter Section House & Historic Park Built in 1929 to maintain a section of the railroad, the house serves as Chugach State Park Visitor Center and railroad museum.

Mile 117.4 Potter Marsh Potter Marsh, Anchorage’s most popular wildlife haven, is named after Potter Creek and has formed a well-vegetated and populated marshy habitat. The marsh, although somewhat natural, was originally man-made between 1916 and 1917 when workers built the embankment for the Alaska Railroad.

These embankments (on your left-hand side as you travel into Anchorage) acted as dams, restricting inward tidal flow and preventing the escape of fresh water runoff from the three creeks at the base of the mountains. This process then formed an area of contained water that developed into Potter Marsh.

Each season, thousands of people view the diversity of migrating and nesting birds from the boardwalk viewing area which overlooks the nesting grounds and wildlife refuge area. Some of the hundreds of birds that visit the marsh each season include the whi stli ng and trumpeter swans, ducks, shorebirds, grebes, marsh hawks, bald eagles, mew gulls, and arctic terns. Most of the birds will summer here and fly south to Mexico and South America for the winter.

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